SINIAN SYSTEM IN CHINA AND ITS ANALOGS IN SIBERIA

dc.contributor.author	Khomentovsky V.V.
dc.date.accessioned	2020-12-01T08:37:39Z
dc.date.available	2020-12-01T08:37:39Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=14995730
dc.identifier.citation	Geologiya i geofizika, 1996, , 8, 150-153
dc.identifier.issn	0016-7886
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/20011
dc.description.abstract	There are good grounds to correlate the Lower and Upper Sinian in China with the Baikalian and Yudomian (Vendian) in Siberia, correspondingly. Their comparison, based on event stratigraphy, is corrected by data on stratigraphy of glacier deposits, ediakarian fauna, microfossils, fossil small shells, remains of worm-like organisms, ichnofauna, and stable isotopes. To justify this correlation, the data on the East-European Platform, Finmarken, and Australia are used.
dc.subject	Vendian	en
dc.title	SINIAN SYSTEM IN CHINA AND ITS ANALOGS IN SIBERIA
dc.type	Статья
dc.subject.age	Precambrian::Proterozoic::Neoproterozoic::Vendian	en
dc.subject.age	Докембрий::Протерозой::Неопротерозойская::Вендский	ru

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